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Vôge Plateau
The Vôge plateau is a sandstone plateau in north east France, straddling the departments of Vosges and Haute-Saône, between Vittel, Saint-Loup-sur-Semouse and Remiremont. It covers approximately 700 km² of Lorraine and Franche-Comté, and includes the towns of Xertigny, Darney, and Bains-les-Bains. The region is predominantly agricultural, dotted with valleys and mixed forests, such as oak, beech, and pines. The Faucilles mountains represent the dividing line between the drainage basins of the Mediterranean and the North Sea. The area is irrigated by the river Saône and its early tributaries, and there are many lakes in the region. Vôge is known for its many thermal spas, such as the towns of Bains-les-Bains and Plombières-les-Bains. The architecture is characterised by the use of sandstone as a construction material, notably for garden walls, and flagstone Flagstone (flag) is a generic flat stone, sometimes cut in regular rectangular or square shape and usu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bains-les-Bains
Bains-les-Bains () is a former commune in the Vosges department in Grand Est in eastern France. On 1 January 2017, it was merged into the new commune La Vôge-les-Bains. 5 December 2016 It was the administrative seat of the former Canton of Bains-les-Bains. Geography The river Côney formed the commune's western border.Points of interest * Arboretum de Bains-les-Bains *[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Vosges (department)
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flagstone
Flagstone (flag) is a generic flat stone, sometimes cut in regular rectangular or square shape and usually used for paving slabs or walkways, patios, flooring, fences and roofing. It may be used for memorials, headstones, facades and other construction. The name derives from Middle English ''flagge'' meaning turf, perhaps from Old Norse ''flaga'' meaning slab or chip. Flagstone is a sedimentary rock that is split into layers along bedding planes. Flagstone is usually a form of a sandstone composed of feldspar and quartz and is arenaceous in grain size (0.16 mm – 2 mm in diameter). The material that binds flagstone is usually composed of silica, calcite, or iron oxide. The rock color usually comes from these cementing materials. Typical flagstone colors are red, blue, and buff, though exotic colors exist. Flagstone is quarried in places with bedded sedimentary rocks with fissile bedding planes. Around the thirteenth century, the ceilings, walls and floors in Eur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plombières-les-Bains
Plombières-les-Bains () is a commune in the Vosges department in Grand Est in eastern France. It was the seat of the former canton of Plombières-les-Bains. ''Les bains'' refers to the hot springs in the area, whose properties were first discovered by the Romans. In succeeding centuries, its baths were visited by Montaigne, Voltaire, the Dukes of Guise, the Dukes of Lorraine, Beaumarchais, Napoleon Bonaparte, Joséphine de Beauharnais, Napoléon III, Berlioz, Lamartine and Alfred de Musset. It is still a spa town with many buildings from the Second French Empire including the Church Saint Amé built with the financial support of Napoléon III. Plombières Agreement The "Pavilion of the Princes" at Plombières, was renamed following the meeting on 21 July 1858 between Napoleon III and Camillo Benso, Count of Cavour, who secretly negotiated the “ Plombières Agreement” as they sat alone together in a small horse-drawn carriage slowly progressing round and round the t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saône
The Saône ( , ; frp, Sona; lat, Arar) is a river in eastern France. It is a right tributary of the Rhône, rising at Vioménil in the Vosges department and joining the Rhône in Lyon, at the southern end of the Presqu'île. The name derives from that of the Gallic river goddess Souconna, which has also been connected with a local Celtic tribe, the Sequanes. Monastic copyists progressively transformed ''Souconna'' to ''Saoconna'', which ultimately gave rise to . The other recorded ancient names for the river were and . Geography The Saône rises at Vioménil at the foot of the cliff of the Faucilles in the Vosges at an elevation of , and flows into the Rhône at Lyon at an elevation of . Its length is . Its largest tributary is the Doubs; upstream of receiving the Doubs at Verdun-sur-le-Doubs in Saône-et-Loire, the Saône is called the "Petite Saône" (lesser Saône), which reflects the large contribution of the Doubs to the Saône. In fact the Doubs' mean annual fl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Darney
Darney () is a commune in the Vosges department in Grand Est in northeastern France. It is located in the Vôge Plateau, around the location of the source of the river Saône. Darney is known for its forest of oak and beech trees. History Darney is built on a promontory dominating the valley of the Saône. The Romans built a castle here to control the area, and watch the forested countryside. As a fortified town in the Middle Ages, Darney had towers and two fortified gates, and was known as the "city of thirty towers". Theobald II, Duke of Lorraine gave the town its church in 1308. The town suffered during the Thirty years war, being razed by the Swedes led by Bernard of Saxe-Weimar, who were allies of the French, in 1634. The castle of the time was destroyed in 1639. Remnants of this castle still exist, as well as the current, smaller castle, which was built in 1725. During the First World War, Darney was the rallying point for Czech and Slovak volunteers, where they ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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